Enhancing spatial resolution of GRACE-derived groundwater storage anomalies in Urmia catchment using machine learning downscaling methods

被引:18
|
作者
Sabzehee, F. [1 ]
Amiri-Simkooei, A. R. [1 ,2 ]
Iran-Pour, S. [1 ]
Vishwakarma, B. D. [3 ,4 ,5 ]
Kerachian, R. [6 ]
机构
[1] Univ Isfahan, Fac Civil Engn & Transportat, Dept Geomat Engn, Esfahan 73441, Iran
[2] Delft Univ Technol, Dept Geosci & Remote Sensing, NL-2600 AA Delft, Netherlands
[3] Indian Inst Sci, Interdisciplinary Ctr Water Res, Bangalore 560012, India
[4] Indian Inst Sci, Ctr Earth Sci, Bangalore 560012, India
[5] Univ Bristol, Sch Geog Sci, Bristol BS8 1RL, England
[6] Univ Tehran, Coll Engn, Sch Civil Engn, Tehran, Iran
关键词
Groundwater storage; Downscaling methods; Urmia catchment; GRACE; Machine learning; Mann-kendall test; NEURAL-NETWORK MODELS; WATER STORAGE; TREND ANALYSIS; HYDROLOGICAL MODELS; SOIL-MOISTURE; RIVER-BASIN; LAKE BASIN; CLIMATE; ASSIMILATION; VARIABILITY;
D O I
10.1016/j.jenvman.2022.117180
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Urmia lake in north-west Iran has dried up to perilously low levels in the past two decades. In this study, we investigate the drivers behind the decline in lake water level with the help of in-situ and remote sensing data. We use total water storage (TWS) changes from the gravity recovery and climate experiment (GRACE) satellite mission. TWS from GRACE includes all the water storage compartments in a column and is the only remote sensing product that can help in estimating groundwater storage (GWS) changes. The coarse spatial (approx. 300 km) resolution of GRACE does not allow us to identify local changes that may have led to the Urmia lake disaster. In this study, we tackle the poor resolution of the GRACE data by employing three machine learning (ML) methods including random forest (RF), support vector regression (SVR) and multi-layer perceptron (MLP). The methods predict the groundwater storage anomaly (GWSA), derived from GRACE, as a function of hydro-climatic variables such as precipitation, evapotranspiration, land surface temperature (LST) and normalized difference vegetation index (NDVI) on a finer scale of 0.25 degrees x 0.25 degrees. We found that i) The RF model exhibited highest R (0.98), highest NSE (0.96) and lowest RMSE (18.36 mm) values. ii) The RF downscaled data indicated that the exploitation of groundwater resources in the aquifers is the main driver of groundwater storage and changes in the regional ecosystem, which has been corroborated by few other studies as well. The impact of precipitation and evapotranspiration on the GWSA was found to be rather weak, indicating that the anthropogenic derivers had the most significant impact on the GWSA changes. iii) We generally observed a significant negative trend in GWSA, having also significant positive correlations with the well data. However, over regions with dam con-struction significant negative correlations were found.
引用
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页数:16
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